天然土壤有机质中菲的分配行为

Distribution Behaviors of Phenanthrene to Humic Fractions in Natural Soil

天然土壤吸附不同初始浓度的菲后,提取胡敏酸组分(包括胡敏酸和富里酸),通过计算得到胡敏素组份所吸附的菲,用以研究菲在2种组份中的动态吸附/分配行为,以及初始浓度的影响,并利用Freundlich式进行拟合.结果表明:天然土壤中菲的吸附/分配过程表现出分阶段特征:从最初的快吸附至48 h左右达到转折点,然后进入慢吸附过程.在快吸附至转折点阶段,胡敏酸组分中菲的吸附比例(吸附量与初始量之比)出现先升后降的波动,可归因于初始时段矿物表面吸附、胡敏素竞争吸附的影响.在慢吸附阶段,胡敏酸中菲的吸附比例变化很小,菲初始浓度的影响也不大;而对于胡敏素组份,低初始浓度条件下菲的吸附比例明显大于高初始浓度条件,并呈现逐步增加的趋势,表明胡敏素组份是慢吸附的主要发生域.模型参数拟合结果显示:胡敏酸、全土、胡敏素吸附的非线性程度依次增加,并随时间逐渐加强.在吸附/分配的动力学过程中,胡敏酸和胡敏素分阶段不同的变化特征反映出土壤有机质组分异质性对非线性吸附行为的影响.

After adsorption of phenanthrene by the natural soil under different concentrations initially added, the soil sample was extracted for humic acid fraction （including humic acid and fulvic acid）, and the sorption amount of phenanthrene in humin fraction was calculated to investigate the adsorption/distrlbution kinetics in two soil organic fractions and the corresponding influence of original phenanthrene concentration. The experimental data were fitted using Freundlich equation. The results show that, distribution of phenanthrene in the soil exhibited a multl-stage property, i.e., from a first fast sorption to a breakthrough at about 48 h, then followed by a slow sorption procedure. In the fast sorption stage （before 48 h）, there was an up-to-down fluctuation of phenanthrene sorption ratio （sorption amount/added amount） in humic acid fraction, possibly due to surface sorption by minerals and competitive sorption by humin fraction. In the slow sorption stage, variations in sorption ratio in humic acid fraction was very small, and the influence of original concentration of phenanthrene was slight ; while for humin fraction, the sorption ratio of phenanthrene at lower initial concentration was significantly higher than at higher one, in addition, the sorption ratio showed a gradually increasing trend, indicated humin fraction as the main domain in charge of the slow sorption. The fitting results of model parameters demonstrated that, sorption nonlinearity of phenanthrene in the natural soil increased in the following order： humic acid fraction〈 whole soil〈 humin fraction, and enhanced gradually. Different characteristics of humic acid and humin fractions in the multi-stage kinetics of phenanthrene sorption/distribution further reflected the effects of heterogenerity of soil organic fractions on nonlinear sorption behaviors.